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Fig. 3


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Below the surface velocity inversions, MURaM-QS dataset. Patches of 125 by 125 pixels2 extracted from instantaneous transverse velocity field maps which were computed at geometrical depths (top) d = 0 km, (middle) d = 144 km, (bottom) d = 560 km by (left column) the MURaM-QS simulation (Vögler et al., 2005) and (middle column) single-layer output versions of DeepVel. The divergence of the transverse plasma motions (i.e., t·vt) is displayed as colored background to emphasize the complexity of the structures that arise at increasing depths. (Right column) Scatterplots comparing amplitudes ||vD,t|| to ||vref,t|| at each geometrical depth. The black line represents the expected solution (i.e., a coefficient of determination R2 = 1).

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